Page 104 - General Knowledge
P. 104

GENERAL KNOWLEDGE                                                                               2019



              There are two important layers in the ionosphere viz. E layer or Kennelly Heavy side layer
                that reflects the medium radio waves, thus helping in short distance radio communication
                and F layer or Appleton layer that reflects the short radio waves and helps in long distance
                radio communication.
              The outermost layer of the Earth‘s atmosphere is known as the Exosphere. It is so highly
                rarefied a region that its boundary is not clear.
            Lithosphere
              The lithosphere is an  Earth‘s  outermost  layer,  composed  of  rocks in  the  crust  and  upper
                mantle that behave as brittle solids.
              The rigid lithosphere sits on the top of the asthenosphere, a layer of the mantle in which
                rocks are hot and deformable.
              The lithosphere is the solid, rocky crust covering the entire planet. This crust is inorganic and

                is composed of minerals.
              It covers the entire surface of the earth from the top of Mount Everest to the bottom of the
                Mariana Trench.
              The actual thickness of the lithosphere varies considerably, and can range from roughly 40
                km to 280 km.
              Earth‘s lithosphere includes the crust and the uppermost mantle, which constitute the hard
                and rigid outer layer of the Earth.
              The lithosphere is subdivided into tectonic plates.
              The  lithosphere  ends  at  the  point  when  the  minerals  in  the  earth‘s  crust  begin  to
                demonstrate viscosity and fluid behaviors.
            Rocks
              The earth‘s crust is formed of mineral materials called rocks.
              The  rocks  which  form  the  substructure  of  our  lithosphere  are  grouped  into  three  broad
                categories:

            Igneous Rocks
              Igneous rocks are formed by the solidification of molten magma from the interior of the earth.
              About 95% of the earth‘s crust is made of this type of rock. In fact, all other types of rocks
                originate from these rocks, and therefore, they are also called primary rocks.
              Igneous rocks are of three types.

            Characteristics of Igneous Rocks

              The igneous rock does not contain layers.
              They are without fossils and the upper part of the rock contains joints.
              They are formed by volcanic lava.
              They are crystalline rocks and impervious rocks.
              They are massive and the weathering effect is difficult over them.
              They are primary rocks of the crust, hence are also called the primary rocks.

            Sedimentary Rocks
              These rocks are formed from the sediment deposits on the ocean beds.
              They  comprise  only about  5%  of  the earth‘s  crust,  but  cover  about  75%  of  the  total land
                surface.



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